Question 11.2: Solve the example problem in Sec. 11.5.4, but assume that th...
Solve the example problem in Sec. 11.5.4, but assume that the seismic zone = 1. Compare the results with the solution to the example problem in Sec. 11.5.4.
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Use the following data: soil profile type = S _{ C } and seismic zone = 1.
1. Seismic coefficient C_{a} (Table 11.2): Entering Table 11.2 with soil profile type C_{C} and zone 1, the value of C_{a} = 0.09.
2. Seismic coefficient C_{v} (Table 11.5): Entering Table 11.5 with soil profile type S_{C} and zone 1, the value of C_{v} = 0.13.
3. Values of T_{s} \text { and } T_{0} [Eqs. (11.5) and (11.6)]: The values of T_{s} \text { and } T_{0} can be calculated as follows:
T_{S}=\frac{C_{v}}{2.5 C_{a}}=\frac{0.13}{2.5(0.09)}=0.58 s
T_{0}=0.2 T_{s}=0.20(0.58)=0.12 s
By using Fig. 11.10 and the values C_{a}=0.09, C_{v}=0.13, T_{s}=0.58 s , \text { and } T_{0}=0.12 s, the response spectrum can be determined and is shown in Fig. 11.20.
TABLE 11.2 Seismic Coefficient C_{a} | |||||
Soil profile type | Seismic zone (see Fig. 5.17) | ||||
Zone 1 | Zone 2A | Zone 2B | Zone 3 | Zone 4 | |
S_{A} | 0.06 | 0.12 | 0.16 | 0.24 | 0.32 N_{a} |
S_{B} | 0.08 | 0.15 | 0.20 | 0.30 | 0.40 N_{a} |
S_{C} | 0.09 | 0.18 | 0.24 | 0.33 | 0.40 N_{a} |
S_{D} | 0.12 | 0.22 | 0.28 | 0.36 | 0.44 N_{a} |
S_{E} | 0.19 | 0.30 | 0.34 | 0.36 | 0.44 N_{a} |
S_{F} | Soil requiring a site-specific evaluation (see Sec. 11.5.2) |
TABLE 11.5 Seismic Coefficient C_{v} | ||||||
Soil profile type | Seismic zone (see Fig. 5.17) | |||||
Zone 1 | Zone 2A | Zone 2B | Zone 3 | Zone 4 | ||
S_{A} | 0.06 | 0.12 | 0.16 | 0.24 | 0.32 N_{v} | |
S_{B} | 0.08 | 0.15 | 0.20 | 0.30 | 0.40 N_{v} | |
S_{C} | 0.13 | 0.25 | 0.32 | 0.45 | 0.56 N_{v} | |
S_{D} | 0.18 | 0.32 | 0.40 | 0.54 | 0.64 N_{v} | |
S_{E} | 0.26 | 0.50 | 0.64 | 0.84 | 0.96 N_{v} | |
S_{F} | Soil requiring a site-specific evaluation (see Sec. 11.5.2) | |||||
Data obtained from the Uniform Building Code (1997). Obtain N_{v} from Table 11.6. |
TABLE 11.6 Near-Source Factor N_{v} | ||||
Seismic source type (see Table 11.4) | Closest distance to known seismic source | |||
≤ 1.2mi (≤2 km) | 3 mi (5 km) | 6 mi (10 km) | ≥ 9 mi (≥ 15 km) | |
A | 2.0 | 1.6 | 1.2 | 1.0 |
B | 1.6 | 1.2 | 1.0 | 1.0 |
C | 1.0 | 1.0 | 1.0 | 1.0 |
Notes: Data obtained from the Uniform Building Code (1997). Near-source factor N_{v} is only needed if the seismic zone = 4 (see Table 11.5). The near-source factor may be based on the linear interpolation of values for distances other than those shown in the table. The location and type of seismic sources to be used for design can be based on geologic data, such as recent mapping of active faults by the U.S. Geological Survey or the California Division of Mines and Geology. The closest distance to the known seismic source can be calculated as the minimum distance between the site and the surface location of the fault plane (or the surface projection of the fault plane). If there are several sources of seismic activity, then the closest one to the site should be considered to be the governing case. |
TABLE 11.4 Seismic Source Type | |||
Seismic source type | Seismic source definition | ||
Seismic source description | Maximum moment magnitude M_{w} ≥ 7 | Slip rate, mm/yr | |
A | Faults that are capable of producing large-magnitude events and that have a high rate of seismic activity | M_{w} ≥ 7 | SR ≥ 5 |
B | All faults other than types A and C | M_{w} ≥ 7 | SR < 5 |
M_{w} < 7 | SR > 2 | ||
M_{w} ≥ 6.5 | SR < 2 | ||
C | Faults that are not capable of producing large-magnitude earthquakes and that have a relatively low rate of seismic activity | M_{w} < 6.5 | SR ≤ 2 |
Notes: Data obtained from the Uniform Building Code (1997). Seismic source type is only needed if the seismic zone = 4 (see Table 11.2). Subduction sources shall be evaluated on a site-specific basis. For the seismic source definition, both the maximum moment magnitude M_{w} and slip rate (SR) conditions must be satisfied concurrently when determining the seismic source type. |


